波兰盆地二叠纪和三叠纪地层生烃模拟:对油气潜力评价的启示

IF 0.9 4区 地球科学 Q3 GEOLOGY
D. Botor
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引用次数: 0

摘要

主要的Do - lo在ba - sin轴上达到接近100%的值。由于埋深较浅,上三叠统烃源岩的TR值普遍低于泽赫施泰因主侏罗组烃源岩。Up per Tri - sic烃源岩沿ba - sin轴的TR值最高,在Pi³a IG 1钻孔和Piotrków Trybunalski IG 1钻孔之间,其中Kroœniewice槽(Kroœniewice IG 1钻孔和Budziszewice IG 1钻孔之间)的TR值最高,达到> - 90%。三叠世晚期至中侏罗世早期,捷克斯坦主坳陷和上三叠统分别进入含油窗口。烃源岩的生烃活动一直持续到晚第三纪,并于晚第三纪中期完成生烃活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrocarbon generation modelling in the Permian and Triassic strata of the Polish Basin: implications for hydrocarbon potential assessment
Main Do lo mite reached val ues ap proach ing 100% along the ba sin axis. The TR in the Up per Tri as sic source rocks is gen er ally lower than in the Zechstein Main Do lo mite due to lesser burial. The Up per Tri as sic source rocks have the high est TR val ues (>50%) along the ba sin axis, in the area be tween bore holes Pi³a IG 1 and Piotrków Trybunalski IG 1, with the most pro nounced zone in the Kroœniewice Trough (i.e., be tween the Kroœniewice IG 1 and Budziszewice IG 1 bore holes), where the TR reached >90%. The Zechstein Main Do lo mite and Up per Tri as sic en tered the oil win dow in the Late Tri as sic to Early–Mid dle Ju ras sic, re spec tively. Hydrocarbon gen er a tion con tin ued un til the Late Cre ta ceous, and was com pleted dur ing tec tonic in ver sion of the ba sin.
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来源期刊
Geological Quarterly
Geological Quarterly 地学-地质学
CiteScore
2.20
自引率
0.00%
发文量
19
审稿时长
>12 weeks
期刊介绍: The policy of the Geological Quarterly is to publish significant contributions of information and geological insight relevant to an international readership. The journal has been issued since 1957 at the Polish Geological Institute - National Research Institute and, at present, is the leading Earth sciences journal in Poland. All aspects of Earth and related sciences, and universal and broad regional rather than locally oriented topics are covered. The journal is intended to be an international forum for the exchange of information and ideas, particularly on important geological topics of Central Europe.
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